Boletín de aludes

Southeast Mountains

Crested Butte Avalanche Center
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Peligro de aludes

Sun
Alta montaña
2 · Moderado
Límite del bosque
2 · Moderado
Bajo el límite
2 · Moderado
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Desactualizado: este boletín caducó 3 years ago. Estás viendo condiciones pasadas, no el boletín vigente.

Lo esencial

Skiers and riders have been finding the safest riding and best powder where the snowpack is deep and protected from the sun and wind on northerly aspects.   This week, several large natural and triggered avalanches have occurred in wind-drifted terrain or as you move towards sunnier terrain (east or west facing) where there are several recently buried problematic crusts.  Stay cautious of sunbaked slopes once surface crusts thaw.  This video summarizes most of the dangerous avalanche activity we saw this week.    

Problemas de aludes

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    2–3

    There are several faceted weak layers in the snowpack that remain a concern in some terrain. The most concerning slopes include those that held an unusually shallow and weak snowpack prior to our March storms (like Round Mountain), where snow depths are currently less than about 5 feet (150cm) deep, or in wind-effected terrain with variable snow depths (like Teo).  There are also recently buried faceted crusts in the upper snowpack on easterly and westerly-facing slopes that are just developing an issue (like Whetstone). Carefully assess the snowpack structure and give yourself a margin for error in handling this problem. There is a high degree of variability across the region and on different aspects. Opt for mellower slope angles when in doubt.  

     

    A persistent slab in the Anthracites ran midweek.   

  • Storm Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–2

    Our midweek storm formed storm slabs more than a foot thick on drifted terrain.  The threat of new snow instabilities is diminishing now that we are three days from the storm.  The most concerning slopes are at higher elevations where drifting caused slabs to be thicker and denser, or on very steep rollovers below treeline.  Additionally, watch for shallow sluffs on shady aspects and loose wet avalanches to develop on the southern half of the compass once surface crusts thaw into mushy snow.  

    A large storm slab in Wolverine Basin in terrain where winds stiffened the recent storm snow.  

Avalanche Discussion

The oscillating pattern of large winter storms and subsequent warmups have created challenging avalanche conditions, and backcountry traveleris continue to get surprised.  Another large slab was triggered yesterday on Mt. Justice on an easterly aspect.  The eastern quadrant has been the bullseye for large avalanches this week.  There are several buried crusts in the upper snowpack that are giving irregular but dangerous feedback, including these D2.5 and D3 avalanches near Marble, this D2.5 avalanche in the Anthracites, and this D2 on Mt. Axtell.  Our March 10th interface, at the base of our two big storms a few feet deep, has been most productive in shallow areas, demonstrated in this video, or wind-protected/leeward slopes where thin faceted crusts developed during our early March dry spell, described in this video.  Our forecast team has been looking for the same issue on northerly aspects lacking a crust without success, although I suspect you could find the issue on an unusually shallow or rocky slope, particularly along the southern boundary of our forecast area.  The most recent facet/crust layer (3/15) is buried about a foot deep on the same aspects, and evolving from a storm slab issue to a persistent slab issue. We believe this issue spans all elevations because it formed during a period without much wind damage. Thus, I'm expanding the rose today to account for the issue persisting into the next round of storms as this week's storm slabs phase off the list, potentially by tomorrow. 

Issues on the southern half of the compass will be driven by surface warming today.  While crusts are frozen this morning, you have a lower likelihood of triggering a slab and no concerns for wet loose activity.  Once the snow surface becomes soft and mushy, instabilities will be more likely.  Time your travels into steep terrain accordingly.  

In summary, there seem to be more issues on sun-warmed slopes due to buried crusts and warming-related slab consolidation or wet activity.  The powder is higher quality on the coldest aspects and has been less active except for in drifted terrain, like this slide in Wolverine Basin.  

Events:  The Al Johnson race is Sunday, March 19. Information and registration are here.  Day of race registration and bib pick up 9-11 a.m. at the Adventure Center in Mountaineer Square. Proceeds go to the CBAC.

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